Atmospheric Pressure given Total or Absolute Pressure Solution

STEP 0: Pre-Calculation Summary
Formula Used
Atmospheric pressure = Absolute pressure-(Mass Density*[g]*Wave Height*cosh(2*pi*(Distance above the Bottom)/Wavelength))*cos(Phase Angle)/(2*cosh(2*pi*Water Depth/Wavelength))+(Mass Density*[g]*Seabed Elevation)
Patm = Pabs-(ρ*[g]*H*cosh(2*pi*(DZ+d)/λ))*cos(θ)/(2*cosh(2*pi*d/λ))+(ρ*[g]*Z)
This formula uses 2 Constants, 2 Functions, 9 Variables
Constants Used
[g] - Gravitational acceleration on Earth Value Taken As 9.80665
pi - Archimedes' constant Value Taken As 3.14159265358979323846264338327950288
Functions Used
cos - Cosine of an angle is the ratio of the side adjacent to the angle to the hypotenuse of the triangle., cos(Angle)
cosh - The hyperbolic cosine function is a mathematical function that is defined as the ratio of the sum of the exponential functions of x and negative x to 2., cosh(Number)
Variables Used
Atmospheric pressure - (Measured in Pascal) - Atmospheric pressure also known as barometric pressure (after the barometer), is the pressure within the atmosphere of Earth.
Absolute pressure - (Measured in Pascal) - Absolute pressure is the sum of gauge pressure and atmospheric pressure.
Mass Density - (Measured in Kilogram per Cubic Meter) - The Mass Density of a substance is its mass per unit volume.
Wave Height - (Measured in Meter) - Wave Height of a surface wave is the difference between the elevations of a crest and a neighboring trough.
Distance above the Bottom - (Measured in Meter) - Distance above the Bottom expressing the local fluid velocity component.
Wavelength - (Measured in Meter) - Wavelength can be defined as the distance between two successive crests or troughs of a wave.
Phase Angle - (Measured in Radian) - Phase Angle characteristic of a periodic wave. The angular component periodic wave is known as the phase angle. It is a complex quantity measured by angular units like radians or degrees.
Water Depth - (Measured in Meter) - Water Depth of the considered catchment. Water depth means the depth as measured from the water level to the bottom of the considered water body.
Seabed Elevation - Seabed Elevation of the catchment under consideration. Seabed is the bottom of the ocean.
STEP 1: Convert Input(s) to Base Unit
Absolute pressure: 534000 Pascal --> 534000 Pascal No Conversion Required
Mass Density: 997 Kilogram per Cubic Meter --> 997 Kilogram per Cubic Meter No Conversion Required
Wave Height: 3 Meter --> 3 Meter No Conversion Required
Distance above the Bottom: 2 Meter --> 2 Meter No Conversion Required
Wavelength: 26.8 Meter --> 26.8 Meter No Conversion Required
Phase Angle: 30 Degree --> 0.5235987755982 Radian (Check conversion here)
Water Depth: 1.05 Meter --> 1.05 Meter No Conversion Required
Seabed Elevation: 0.8 --> No Conversion Required
STEP 2: Evaluate Formula
Substituting Input Values in Formula
Patm = Pabs-(ρ*[g]*H*cosh(2*pi*(DZ+d)/λ))*cos(θ)/(2*cosh(2*pi*d/λ))+(ρ*[g]*Z) --> 534000-(997*[g]*3*cosh(2*pi*(2)/26.8))*cos(0.5235987755982)/(2*cosh(2*pi*1.05/26.8))+(997*[g]*0.8)
Evaluating ... ...
Patm = 528116.164890089
STEP 3: Convert Result to Output's Unit
528116.164890089 Pascal --> No Conversion Required
FINAL ANSWER
528116.164890089 528116.2 Pascal <-- Atmospheric pressure
(Calculation completed in 00.020 seconds)

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Coorg Institute of Technology (CIT), Coorg
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16 Pressure Component Calculators

Water Surface Elevation of Two Sinusoidal Wave
Go Elevation of Water Surface = (Wave Height/2)*cos((2*pi*Spatial (Progressive Wave)/Wavelength of Component Wave 1)-(2*pi*Temporal (Progressive Wave)/Wave Period of Component Wave 1))+(Wave Height/2)*cos((2*pi*Spatial (Progressive Wave)/Wavelength of Component Wave 2)-(2*pi*Temporal (Progressive Wave)/Wave Period of Component Wave 2))
Phase Angle for Total or Absolute Pressure
Go Phase Angle = acos((Absolute Pressure+(Mass Density*[g]*Seabed Elevation)-(Atmospheric Pressure))/((Mass Density*[g]*Wave Height*cosh(2*pi*(Distance above the Bottom)/Wavelength))/(2*cosh(2*pi*Water Depth/Wavelength))))
Atmospheric Pressure given Total or Absolute Pressure
Go Atmospheric pressure = Absolute pressure-(Mass Density*[g]*Wave Height*cosh(2*pi*(Distance above the Bottom)/Wavelength))*cos(Phase Angle)/(2*cosh(2*pi*Water Depth/Wavelength))+(Mass Density*[g]*Seabed Elevation)
Total or Absolute Pressure
Go Absolute pressure = (Mass Density*[g]*Wave Height*cosh(2*pi*(Distance above the Bottom)/Wavelength)*cos(Phase Angle)/2*cosh(2*pi*Water Depth/Wavelength))-(Mass Density*[g]*Seabed Elevation)+Atmospheric Pressure
Dynamic Component due to Acceleration from Absolute Pressure Equation
Go Dynamic Component due to Acceleration = (Mass Density*[g]*Wave Height*cosh(2*pi*(Distance above the Bottom)/Wavelength))*cos(Phase Angle)/(2*cosh(2*pi*Water Depth/Wavelength))
Height of Surface Waves based on Subsurface Measurements
Go Elevation of Water Surface = Correction Factor*(Pressure+(Mass Density*[g]*Depth below the SWL of Pressure Gauge))/(Mass Density*[g]*Pressure Response Factor)
Correction Factor given Height of Surface Waves based on Subsurface Measurements
Go Correction Factor = Elevation of Water Surface*Mass Density*[g]*Pressure Response Factor/(Pressure+(Mass Density*[g]*Depth below the SWL of Pressure Gauge))
Depth below SWL of Pressure Gauge
Go Depth below the SWL of Pressure Gauge = ((Elevation of Water Surface*Mass Density*[g]*Pressure Response Factor/Correction Factor)-Pressure)/Mass Density*[g]
Friction Velocity given Dimensionless Time
Go Friction Velocity = ([g]*Time for Dimensionless Parameter Calculation)/Dimensionless Time
Water Surface Elevation
Go Elevation of Water Surface = (Wave Height/2)*cos(Phase Angle)
Wave celerity for shallow water given water depth
Go Celerity of the Wave = sqrt([g]*Water Depth)
Atmospheric Pressure given Gauge Pressure
Go Atmospheric Pressure = Absolute Pressure-Gauge Pressure
Total Pressure given Gauge Pressure
Go Total Pressure = Gauge Pressure+Atmospheric Pressure
Water Depth given Wave Celerity for Shallow Water
Go Water Depth = (Celerity of the Wave^2)/[g]
Radian Frequency given Wave Period
Go Wave Angular Frequency = 1/Mean Wave Period
Wave Period given average Frequency
Go Wave Period = 1/Wave Angular Frequency

Atmospheric Pressure given Total or Absolute Pressure Formula

Atmospheric pressure = Absolute pressure-(Mass Density*[g]*Wave Height*cosh(2*pi*(Distance above the Bottom)/Wavelength))*cos(Phase Angle)/(2*cosh(2*pi*Water Depth/Wavelength))+(Mass Density*[g]*Seabed Elevation)
Patm = Pabs-(ρ*[g]*H*cosh(2*pi*(DZ+d)/λ))*cos(θ)/(2*cosh(2*pi*d/λ))+(ρ*[g]*Z)

What is Wavelength?

Wavelength, distance between corresponding points of two consecutive waves. “Corresponding points” refers to two points or particles in the same phase i.e., points that have completed identical fractions of their periodic motion.

How to Calculate Atmospheric Pressure given Total or Absolute Pressure?

Atmospheric Pressure given Total or Absolute Pressure calculator uses Atmospheric pressure = Absolute pressure-(Mass Density*[g]*Wave Height*cosh(2*pi*(Distance above the Bottom)/Wavelength))*cos(Phase Angle)/(2*cosh(2*pi*Water Depth/Wavelength))+(Mass Density*[g]*Seabed Elevation) to calculate the Atmospheric pressure, The Atmospheric Pressure given Total or Absolute Pressure is the pressure of having no matter inside a space, or a perfect vacuum. Measurements taken in absolute pressure use this absolute zero as their reference point. Atmospheric pressure is denoted by Patm symbol.

How to calculate Atmospheric Pressure given Total or Absolute Pressure using this online calculator? To use this online calculator for Atmospheric Pressure given Total or Absolute Pressure, enter Absolute pressure (Pabs), Mass Density (ρ), Wave Height (H), Distance above the Bottom (DZ+d), Wavelength (λ), Phase Angle (θ), Water Depth (d) & Seabed Elevation (Z) and hit the calculate button. Here is how the Atmospheric Pressure given Total or Absolute Pressure calculation can be explained with given input values -> 528078.2 = 534000-(997*[g]*3*cosh(2*pi*(2)/26.8))*cos(0.5235987755982)/(2*cosh(2*pi*1.05/26.8))+(997*[g]*0.8).

FAQ

What is Atmospheric Pressure given Total or Absolute Pressure?
The Atmospheric Pressure given Total or Absolute Pressure is the pressure of having no matter inside a space, or a perfect vacuum. Measurements taken in absolute pressure use this absolute zero as their reference point and is represented as Patm = Pabs-(ρ*[g]*H*cosh(2*pi*(DZ+d)/λ))*cos(θ)/(2*cosh(2*pi*d/λ))+(ρ*[g]*Z) or Atmospheric pressure = Absolute pressure-(Mass Density*[g]*Wave Height*cosh(2*pi*(Distance above the Bottom)/Wavelength))*cos(Phase Angle)/(2*cosh(2*pi*Water Depth/Wavelength))+(Mass Density*[g]*Seabed Elevation). Absolute pressure is the sum of gauge pressure and atmospheric pressure, The Mass Density of a substance is its mass per unit volume, Wave Height of a surface wave is the difference between the elevations of a crest and a neighboring trough, Distance above the Bottom expressing the local fluid velocity component, Wavelength can be defined as the distance between two successive crests or troughs of a wave, Phase Angle characteristic of a periodic wave. The angular component periodic wave is known as the phase angle. It is a complex quantity measured by angular units like radians or degrees, Water Depth of the considered catchment. Water depth means the depth as measured from the water level to the bottom of the considered water body & Seabed Elevation of the catchment under consideration. Seabed is the bottom of the ocean.
How to calculate Atmospheric Pressure given Total or Absolute Pressure?
The Atmospheric Pressure given Total or Absolute Pressure is the pressure of having no matter inside a space, or a perfect vacuum. Measurements taken in absolute pressure use this absolute zero as their reference point is calculated using Atmospheric pressure = Absolute pressure-(Mass Density*[g]*Wave Height*cosh(2*pi*(Distance above the Bottom)/Wavelength))*cos(Phase Angle)/(2*cosh(2*pi*Water Depth/Wavelength))+(Mass Density*[g]*Seabed Elevation). To calculate Atmospheric Pressure given Total or Absolute Pressure, you need Absolute pressure (Pabs), Mass Density (ρ), Wave Height (H), Distance above the Bottom (DZ+d), Wavelength (λ), Phase Angle (θ), Water Depth (d) & Seabed Elevation (Z). With our tool, you need to enter the respective value for Absolute pressure, Mass Density, Wave Height, Distance above the Bottom, Wavelength, Phase Angle, Water Depth & Seabed Elevation and hit the calculate button. You can also select the units (if any) for Input(s) and the Output as well.
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